KLCOA has signed an agreement with the County of Haliburton to adopt a stretch of Kennisis Lake Road from Rough Stone Trail (before West Shore as you’re coming into the lake) to the end of the County Road (at Wilkinson Drive).

Last year’s cleanup was a great success with many volunteers and considerable debris being removed.

We hate to ask but we know for certain that a little effort will leave the roadside looking great for another year. Volunteers are paired up and then given a short stretch of the road. Bags and gloves are provided.

If you can help out for an hour or two the morning of Saturday May 5th, please contact Brenda at b59smith@yahoo.ca. All are welcome. If there’s a student in the family, this is a great way for them to get some of their community volunteer hours. Brenda will provide full details in her response to your email.

Be proud during your drive along Kennisis Road knowing that you had a hand in making the roadside beautiful and free of debris.

As they say, “many hands make light work,” so let’s all come out to help!

Please join us for the KLCOA Members’ Spring Meeting. It is a chance to hear about what has been going on in the community over the winter and what is in store for the coming months. More importantly you will hear a number of presentations related to an issue which affects us all—water quality. And, if you have not done so already, you can renew your KLCOA membership.

Water Levels

The water level on the Kennisis lakes is controlled by a Trent Severn Waterway (TSW) dam where the outflow from our lakes feeds the Kennisis and then the Gull rivers before entering the Trent River.

The TSW uses the Kennisis lakes as a reservoir, lowering the lake in summer to maintain sufficient draught for the main navigation channel on the canal portion of the TSW.

The dam is comprised of nine 12” wooden logs plus a 6” metal “half-log”. With all the logs in place the top of the dam is therefore 9 feet 6 inches above the sill plate of the dam. In recent memory, the TSW leaves 3 logs in place all year resulting in a useable control range of 6 feet 6 inches.

Kennisis Lake Average Water Levels

The following chart records the multi-year average water level (blue line) on Kennisis Lake since 1988. An indication of the potential variability of water levels is provided by the maximum (red line) and minimum (green line) water levels recorded over the same period.

Data provided by the Trent Severn Waterway

How to Read the Chart

Water levels are measured by the Trent Severn Waterway (TSW) using a gauge located at the Kennisis Dam. The water level is measured in metres (m) above the sill plate of the dam.

Key reference points:

Sill plate level 0.00m 0% full

Height of standard stop-log 0.305m

Height of dam with all 9.5 logs in place 2.90m 100% full

TSW Target level in Spring 2.84m 98% full

TSW Winter set level – 3 logs in place 0.92m 32% full

Nominal water level fluctuation 1.92m 66% of capacity

Current Water Level Data

NOTE: While the water level of the lake is ‘controlled’ by the number of logs in the dam, it will rarely be exactly equal to the level of the topmost log in the dam. It is usual for there to be a ‘head’ of water of several centimeters above the top of the dam; it is also possible for the water level of the lake to drop below the level of the topmost log in the dam due to evaporation or the recent addition of a stop-log.

What are the Preferred Water Levels for the Kennisis Lakes?

As a Member of the Coalition for Equitable Water Flow (CEWF), in 2011 the KLCOA identified challenges facing KLCOA members due to the water management practices of the TSW. In particular, we identified problems related to flooding, water access and safe navigation resulting from water level fluctuations.

CEWF is promoting the concept of a lake-specific Preferred Water Level Range during the principal navigation season from mid-May to mid-September.

With the help of data collected by KLCOA Member Doug Lenart, we have focused on the ability to safely navigate between the main lake and Little Kennisis Lake as well as Paddys Bay. This is not the only issue of concern, but it can be quantified with measurable data and solving this issue would also solve other problems. The data collected include a profile of the navigable channels under the bridges as well as clearance and draft specifications for the most common boats found on our lakes. This allows us to calculate the range of water levels that allow for safe navigation between the lakes.

As a result of this analysis, it is proposed is that the TSW be requested to manage the water levels on Kennisis Lake between mid-May and mid-September so that:

The water level not rise above 95% of the full range available for control by the TSW. This is equivalent to a water level that is 4″ below the top of the dam with all logs in place. This level is equal to the multi-year average for early June. Ensuring that the water level did not exceed this upper limit would also help to avoid shoreline erosion and flooding of low-lying properties;

The water level not be allowed to drop below 55% of the TSWs control range. This is equivalent to 51″ below the top of the dam. This level is equal to the multi-year average for September 1st. Ensuring that the water level did not fall below this lower limit would allow safe passage between the lakes, reduce the number of navigation hazards, and also reduce the risk of docks being left high and dry in September.

The overall result would see Kennisis Lake drop about four feet over the summer months instead of five feet as in 2012 or even six feet, as happened in 2007.

KLCOA members supported this approach at the September 2011 AGM, and the information was forwarded to CEWF and then to the TSW along with similar input from other lakes in the Haliburton.

The Preferred Water Level range during the navigation season from May through to Thanksgiving (shaded area between upper and lower preferred limits) – as approved by the KLCOA members

The TSW winter log-set level (purple line) shown for December & January

Note: the left scale is still in metres above the sill plate of the dam:

however the scale increments by 0.3 metres, equivalent to the depth of one of the control logs used to adjust the height of the dam.

From the chart it can be seen that:

the winter-set condition is equal to 3 logs in the dam

the preferred upper limit of 2.75 m for the water level during the navigation season, equivalent to 9 logs in the dam, corresponds to the multi-year average high water level and so should be attainable

the preferred lower limit of 1.6 m for the water level during the navigation season, equivalent to 5 logs in the dam, is typically breached in September, or as early as August in a dry year: however this level has been maintained in the past as shown by the historic maximum. It would appear that this condition could be satisfied most years if the winter-set condition were 4 logs instead of 3

Worked Example

Navigation under the Bridge between Big and Little Kennisis Lakes

Of the 1047 waterfront properties on the Kennisis lakes, 286 are located on Little Kennisis Lake. Navigation between the only marina on the lake and Little Kennisis Lake requires passage under a road bridge. The channel is shallow and there is limited clearance under the bridge. If the water level is too high, some boats do not have sufficient clearance. If the water level is too low there is inadequate draft.

An analysis of the channel profile plus an evaluation of boat characteristics has been conducted. The following is a summary of the findings:

the bottom of the centre of the channel is 0.3 m above the sill plate

the channel profile is a regular ‘shallow-saucer’ shape

assuming the navigational channel occupies 60% of the overall width of the channel there are high-spots that are 0.8 m above the sill plate

the underside of the bridge roadbed is 4.6 m above the sill plate

most boats could pass under the bridge if there was a minimum clearance of 1.8 m

there is thus sufficient clearance at a water level of 2.8 m (close to TSW’s full condition)

most boats require a draft of less than 0.8 m

there should therefore be sufficient draft if the water level is greater than 1.6 m

this allows TSW an operating range during navigation season of 1.2 m (1.6 to 2.8 m or between 5 & 9 logs in)

An environmentally acceptable approach to dredging the channel to remove ‘erratic’ rocks would be desirable and would allow for greater fluctuation in water level without impacting navigation.

Paddy’s Bay Bridge

A second bridge providing access from the main lake to Paddy’s bay has been profiled as well. Although the channel is about 1.0 m above the sill plate and the underside of the roadbed is 4.2 m above the sill plate, it is typically smaller boats that use this channel. No additional water level constraints are therefore deemed essential. Although dredging of the channel would certainly improve access.

Manipulation of 12″ wooden log at TSW dam

The KLCOA is an active member of the Coalition for Equitable Waterflow (CEWF). The CEWF maintains an excellent website with considerable information regarding water levels on lakes feeding the Trent Severn Waterway (TSW).

Through this website the KLCOA endeavours to provide current and timely information regarding water levels for the Kennisis lakes.

Readers looking for historical information about water levels on our lakes or other lakes which feed the TSW are encouraged to use the links provided here to access the CEWF website. The CEWF website also contains a wide variety of briefing notes, member communications reports and presentations regarding water levels and the related complex issues. On the CEWF website the Kennisis lakes information can be found in reports for the Gull River area. If you look at their historical data under the TSW Water Levels category you can access records detailing the average, minimum and maximum water levels for the Kennisis lakes going back to 1988.

In addition there are detailed reports for each of the five most recent years based on data provided by the TSW and Parks Canada. For example, to see a water level chart for 2016, select the 2016 Water Levels Summary, click the link for Gull River and then scroll down to the Kennisis Lake graph. Here is the link to access the CEWF website.